TY  - JOUR
AU  - Feist-Burkhardt, S
AU  - Götz, AE
AU  - Szulc, J
AU  - Borkhataria, R
AU  - Geluk, M
AU  - Haas, János
AU  - Hornung, J
AU  - Jordan, P
AU  - Kempf, O
AU  - Michalík, J
AU  - Nawrocki, J
AU  - Reinhardt, L
AU  - Ricken, W
AU  - Röhling, HG
AU  - Rüffer, T
AU  - Török, Ákos
AU  - Zühlke, R
TI  - Triassic
JF  - CENTRAL EUROPE
J2  - CENTRAL EUROPE
VL  - 2
PY  - 2008
SP  - 749
EP  - 821
PG  - 73
SN  - 1479-0963
UR  - https://m2.mtmt.hu/api/publication/32550094
ID  - 32550094
N1  - Cited By :117            
            Export Date: 12 January 2023
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Török, Ákos
TI  - Controls on development of Mid-Triassic ramps: examples from southern Hungary
JF  - GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS
J2  - GEOL SOC SPEC PUBL
VL  - 149
PY  - 1998
SP  - 339
EP  - 367
PG  - 29
SN  - 0305-8719
DO  - 10.1144/GSL.SP.1999.149.01.16
UR  - https://m2.mtmt.hu/api/publication/1635999
ID  - 1635999
N1  - Cited By :41            
            Export Date: 15 June 2021            
            Correspondence Address: Török, Á.; Department of Geology, Sztoczek u. 2, H-1521 Budapest, Hungary; email: torok@bigmac.eik.bme.hu
AB  - During Mid-Triassic time the palaeogeographical-tectonic setting of the northern Tethyan passive margin and epicontinental basins favoured the ramp morphology, as broad flat areas were available for flooding and establishment of carbonate sedimentation. Throughout this time, in what is now southern Hungary, homoclinal ramps developed, which also exhibit some evidence of partial distal steepening. The nearly 1 km thick Anisian-Ladinian Muschelkalk carbonates are grouped into six depositional units. In each ramp unit facies types were identified representing coastal sabkhas, inner ramp peritidal facies, backshoal lagoons, oolite shoals, storm to fair-weather influenced mid-ramps, proximal to distal shell beds and low-energy outer ramps. Mid- and inner ramp carbonates make up the majority of the successions. The deepest outer ramp facies correspond to the peak transgression of a second-order Triassic sea-level rise. In the Hungarian Muschelkalk three major transgressive-regressive sequences were identified. In Germany, Poland and Spain much thinner and slightly coarser Muschelkalk carbonate successions were formed in the same Mid-Triassic interval. The major sediment redistribution processes were related to storms that generated coquinas, and mud flow deposits. Slow, early diagenesis and the predominance of unstable muddy substrate led to the formation of small-scale slumps, slides and plastic deformation. The fauna reflects the prevalence of carbonate mud and temporarily high-stress conditions. A non 'cool water' origin of this ramp is inferred from the presence of evaporites, early dolomization of inner ramp carbonates, the biota and the palaeogeographical setting. The major controlling factors of Mid-Triassic ramps were the gentle antecedent morphology, the subtropical climate, the high production of carbonate mud and the lack of reef-building organisms, as well as the passive margin setting, which resulted in a moderate and relatively uniform subsidence rate over a wide area.
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Haas, János
AU  - Budai, Tamás
TI  - Upper Permian-Triassic facies zones in the Transdanubian Range
JF  - RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA
J2  - RIV IT PALEON STRATIG
VL  - 101
PY  - 1995
IS  - 3
SP  - 249
EP  - 266
PG  - 18
SN  - 0035-6883
UR  - https://m2.mtmt.hu/api/publication/1019017
ID  - 1019017
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - M, Bleahu
AU  - Mantea, G
AU  - Bordea, S
AU  - Panin, S
AU  - Stefanescu, M
AU  - Sikic, K
AU  - Haas, János
AU  - Kovács, Sándor
AU  - Péró, Csaba
AU  - Bérczi-Makk, A
AU  - Konrád, Gyula
AU  - Nagy, E
AU  - Rálisch-Felgenhauer, E
AU  - Török, Ákos
TI  - Triassic facies types, evolution and paleogeographic relations of the Tisza Megaunit
JF  - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES
J2  - ACTA GEOL HUNG
VL  - 37
PY  - 1994
SP  - 187
EP  - 234
PG  - 48
SN  - 0236-5278
UR  - https://m2.mtmt.hu/api/publication/1025533
ID  - 1025533
LA  - English
DB  - MTMT
ER  -